The Scientific Study of SceneryMethuen & Company, 1900 - 368 страница |
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... feet in length , or twenty leagues , would have made no difference to them ; or , rather , would not have been in any wise conceived or considered by them . Examine the nature of your own emotion ( if you feel it ) at the sight of the ...
... feet in length , or twenty leagues , would have made no difference to them ; or , rather , would not have been in any wise conceived or considered by them . Examine the nature of your own emotion ( if you feel it ) at the sight of the ...
Страница 39
... feet . 4000 to 10,000 " " 25,000 to 30,000 99 The horizontal distribution of different kinds of clouds in space is affected by the time - variations , but over and above this it is specially affected by types of weather , and the ...
... feet . 4000 to 10,000 " " 25,000 to 30,000 99 The horizontal distribution of different kinds of clouds in space is affected by the time - variations , but over and above this it is specially affected by types of weather , and the ...
Страница 58
... feet of superincumbent rock , but they show that under certain conditions rock folding can be produced by slow pressure , and not by rapid movement , and therefore that violent contortion of the strata is by no means proof of rapid ...
... feet of superincumbent rock , but they show that under certain conditions rock folding can be produced by slow pressure , and not by rapid movement , and therefore that violent contortion of the strata is by no means proof of rapid ...
Страница 94
... feet high on a mountain 15,000 feet high may appear as a mere notch at a distance , hardly affecting the general character of the moun- tain outline , but when we are stationed near the base of that cliff it is an object sufficiently ...
... feet high on a mountain 15,000 feet high may appear as a mere notch at a distance , hardly affecting the general character of the moun- tain outline , but when we are stationed near the base of that cliff it is an object sufficiently ...
Страница 96
... feet above the lake of that name . ( See plate in a later chapter . ) Screes which accumu- late at the bottom of a valley often possess an outline similar to that of the curve of water erosion , and as the stream - courses often branch ...
... feet above the lake of that name . ( See plate in a later chapter . ) Screes which accumu- late at the bottom of a valley often possess an outline similar to that of the curve of water erosion , and as the stream - courses often branch ...
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Чести термини и фразе
accordingly accumulation action agents angles barrier basins cause character cliffs clouds coast colour considerable corrasion crater crevasses Crown 8vo crust curve delta Demy 8vo denudation deposits desert regions drainage E. V. LUCAS earth's surface effect erosion escarpment existence extent Fcap feet fissure flow folding formation formed fragments frequently Geological give rise glacial glacier gorge Greenland ground hard rock height Henry Mountains hills hollows horizontal igneous rocks Illustrations islands Lake District land lava limestone lithosphere lower marked mass material monoclinal moraines mountain movement nature névé occupied occur ocean original outline owing particles peneplain plain planes of stratification plateau portion produced result ridge river rocks sand scenery screes Second Edition sediment seen side slope snow soft rocks Spitsbergen strata subaerial subsequent streams Tarn tion tract tributary Ullswater uplift upper valley vapour vegetation vertical volcanic watershed waves weathering wind
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